
sedimentary
Chert (Jasper/Flint variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Dark brown to olive-greenish with mottling; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline (Trigonal); Cleavage: None (has conchoidal fracture); Specific gravity: 2.6 – 2.7.
- Hardness
- 7 (Mohs scale)
- Color
- Dark brown to olive-greenish with mottling
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Dark brown to olive-greenish with mottling; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline (Trigonal); Cleavage: None (has conchoidal fracture); Specific gravity: 2.6 – 2.7.
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolaria) or by chemical precipitation from hydrothermal fluids in marine or groundwater environments. This process often replaces pre-existing sedimentary rocks like limestone.
Uses & applications
Historically used for stone tools and starting fires (flint). Currently used in jewelry (as jasper), as an abrasive, and by collectors. Also used as road surfacing in some regions.
Geological facts
Chert is so hard it can scratch steel. It was one of the most vital materials for prehistoric humans because it fractures like glass into sharp, durable edges suitable for arrowheads and scrapers.
Field identification & locations
Identify in the field by its hardness and its 'conchoidal' (shell-like) fracture pattern. It often feels smooth and slightly greasy/waxy compared to surrounding limestone. Commonly found in riverbeds and limestone outcrops.
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